Extended Data Fig. 2: Global glacier mass projections from the year 2000 until 6000 (% relative to 2020) under an extended 1.5∘C stabilization and 3.0 → 1.5∘C overshoot scenario.
From: Irreversible glacier change and trough water for centuries after overshooting 1.5 °C

Until 2500 the same scenarios as in Fig. 2a were applied. After 2500, an identical climate (randomly repeated climate taken from the last 100 years of the 1.5∘C stabilization scenario) was used. The resulting global mean temperature changes of the extended scenarios are shown. For visual reasons, we only show the simulations until year 6000 as no notable changes occur afterwards, that is the global glacier mass reached steady state in both scenarios.